Yuanyuan Qi, Yating He, Li Yao, Qiuli Yan, Chengyi Wu, Yunpeng Wu, Jinhua Wang
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The results revealed that: (1) The soil water content, alkali-hydrolyzable nitrogen content, and total nitrogen content in the slight rocky desertification area GJ4 were significantly higher than those in the moderate rocky desertification areas KY and MZ3. (2) There were significant differences in the community composition of nitrogen-fixing bacteria across the four rocky desertification areas (R2 = 0.448, P = 0.001). Within the same area, the Shannon index in slight rocky desertification was significantly higher than that of moderate rocky desertification. Rhizobium was the dominant genus. (3) In Gejiu, Yunnan Province, it has been observed that there is a clear negative correlation was observed among rocky desertification grade, soil water content, and nitrogen-fixing bacterial diversity in the typical karst ecosystem. Specifically, intensifying rocky desertification significantly reduces soil moisture and bacterial diversity. The degree of soil rocky desertification, total nitrogen content, total phosphorus content, and pH of soil are the main factors that play a key role in the community composition of the nitrogen-fixing bacteria in the nodules of V. villosa. 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引用次数: 0
摘要
石漠化是喀斯特生态系统中的一种常见现象,对土壤肥力和植被恢复具有重要影响。因此,了解不同石漠化程度下固氮细菌与土壤性质的关系至关重要。本试验旨在研究绒毛弧菌根瘤中固氮细菌的群落结构及影响固氮细菌分布的主要环境因素。基于nifH基因序列分析,我们发现根瘤固氮菌群落组成与石漠化程度显著相关。分析了影响群落组成的土壤理化性质。结果表明:(1)轻度石漠化地区GJ4土壤含水量、碱解氮含量和全氮含量显著高于中度石漠化地区KY和MZ3。(2) 4个石漠化地区固氮细菌群落组成差异显著(R2 = 0.448, P = 0.001)。同一区域内,轻度石漠化的Shannon指数显著高于中度石漠化的Shannon指数。根瘤菌属为优势属。(3)在云南个旧典型喀斯特生态系统中,石漠化程度与土壤含水量、固氮细菌多样性呈明显的负相关关系。具体而言,石漠化加剧显著降低了土壤水分和细菌多样性。土壤石漠化程度、土壤全氮含量、全磷含量和pH值是影响绒毛藤蔓固氮菌群落组成的主要因素。本研究为石漠化治理提供了理论依据。
Relationships between nitrogen-fixing bacteria community structure in Vicia villosa nodules, soil properties and rocky desertification degree in karst area southwest China.
Rocky desertification, a common phenomenon in karst ecosystems, significantly impacts soil fertility and vegetation restoration. Therefore, understanding the relationship between nitrogen-fixing bacteria and soil properties under different degrees of rocky desertification is crucial. Our experiment was conducted to investigate the bacterial community structure and the main environmental factors affecting the distribution of the nitrogen-fixing bacteria in the nodules of V. villosa. Based on nifH gene sequence analysis, we found that the community composition of nitrogen-fixing bacteria in the nodules was significantly correlated with the degree of rocky desertification. The soil physicochemical properties affecting community composition were analyzed. The results revealed that: (1) The soil water content, alkali-hydrolyzable nitrogen content, and total nitrogen content in the slight rocky desertification area GJ4 were significantly higher than those in the moderate rocky desertification areas KY and MZ3. (2) There were significant differences in the community composition of nitrogen-fixing bacteria across the four rocky desertification areas (R2 = 0.448, P = 0.001). Within the same area, the Shannon index in slight rocky desertification was significantly higher than that of moderate rocky desertification. Rhizobium was the dominant genus. (3) In Gejiu, Yunnan Province, it has been observed that there is a clear negative correlation was observed among rocky desertification grade, soil water content, and nitrogen-fixing bacterial diversity in the typical karst ecosystem. Specifically, intensifying rocky desertification significantly reduces soil moisture and bacterial diversity. The degree of soil rocky desertification, total nitrogen content, total phosphorus content, and pH of soil are the main factors that play a key role in the community composition of the nitrogen-fixing bacteria in the nodules of V. villosa. This study provides a theoretical basis for the control of rocky desertification.
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